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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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<strong>Historical</strong> Seismicity and Earthquake Catalogues for Indian Region 343(2) A number of earthquakes have occurred within <strong>the</strong> Indian plate. Many of <strong>the</strong>seare associated with transverse lineaments, which are broadly aligned parallel to <strong>the</strong>movement of <strong>the</strong> Indian plate. Collection of data for earthquakes of M < 5 willenable us to understand <strong>the</strong> extent and activity of <strong>the</strong>se lineaments. Also, <strong>the</strong>y mayreveal <strong>the</strong> relationship between small tremors and bigger shocks, as brought out by<strong>the</strong> preliminary observations <strong>from</strong> <strong>the</strong> new catalogue for peninsular India presentedhere and supported by high-gain port able microseismograph observations.(3) After <strong>the</strong> great Assam earthquake of 1950, <strong>the</strong>re is a relative decrease of seismicactivity in <strong>the</strong> Indian region. With <strong>the</strong> exception of Kinnaur earthquake of January1975, <strong>the</strong> magnitude of earthquakes has rarely exceeded 6.0. This quiescence period,during which strain appears to be accumulating near <strong>the</strong> Indian-Eurasian plateboundary, cautions us to investigate <strong>the</strong> nature of stresses of past earthquakesin greater detail and to study <strong>the</strong> possibility of identifying premonitory changes(Srivastava, 1983).

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